Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP

Abstract In this study, synchronous linkages of the North Sea–Caspian pattern (NCP), associated with large‐scale surface air temperature series selected from National Centers for Environmental Prediction–National Center of Atmospheric Research reanalysis (NCEP‐NCAR) for the region over 50°W–120°E an...

Full description

Bibliographic Details
Published in:International Journal of Climatology
Main Author: Tatli, Hasan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2007
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.1465
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1465
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1465
id crwiley:10.1002/joc.1465
record_format openpolar
spelling crwiley:10.1002/joc.1465 2024-06-02T08:07:37+00:00 Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP Tatli, Hasan 2007 http://dx.doi.org/10.1002/joc.1465 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1465 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1465 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 27, issue 9, page 1171-1187 ISSN 0899-8418 1097-0088 journal-article 2007 crwiley https://doi.org/10.1002/joc.1465 2024-05-03T11:21:46Z Abstract In this study, synchronous linkages of the North Sea–Caspian pattern (NCP), associated with large‐scale surface air temperature series selected from National Centers for Environmental Prediction–National Center of Atmospheric Research reanalysis (NCEP‐NCAR) for the region over 50°W–120°E and 0–80°N are investigated via teleconnection patterns based on phase synchronization. Phase synchronization is the process by which two or more cyclic systems (or subsystems) tend to oscillate with a repeating sequence of relative phase angles. Phase synchronization is usually applied to two waveforms of the same frequency with identical phase angles in each cycle. However, the notion of phase synchronization has been introduced as an extension of classical Huygens' synchronization in the case of interacting chaotic systems if there is an integer relationship of frequency, such that the cyclic systems share a repeating sequence of phase angles over consecutive cycles. The results of the phase synchronization method are compared with those of the classical cross‐correlation method in cases in which cross‐correlation method shows linear spatial cross‐dependency, but the phase synchronization yields nonlinear spatial phase dependency. In the analyses, teleconnection patterns derived from phase synchronization are first calculated for raw and de‐seasoned data (by removing periodic components in the surface air temperature series) in year‐month scale and then for the data in seasonal‐scale (namely, winter, spring, summer and autumn). Teleconnection patterns calculated by phase synchronization improve the experiential intra‐phase relationships between the NCP Index (NCPI) and large‐scale surface air temperature series, and ensures that the major modes of mid and high Northern Hemisphere variability in climate are characterized. Statistically significant phase synchronization patterns related to geopotential dipole heights of the NCPI extending over Greenland, the Balkans, Caspian Sea basin, eastern Mediterranean, Turkey and ... Article in Journal/Newspaper Greenland Wiley Online Library Greenland International Journal of Climatology 27 9 1171 1187
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract In this study, synchronous linkages of the North Sea–Caspian pattern (NCP), associated with large‐scale surface air temperature series selected from National Centers for Environmental Prediction–National Center of Atmospheric Research reanalysis (NCEP‐NCAR) for the region over 50°W–120°E and 0–80°N are investigated via teleconnection patterns based on phase synchronization. Phase synchronization is the process by which two or more cyclic systems (or subsystems) tend to oscillate with a repeating sequence of relative phase angles. Phase synchronization is usually applied to two waveforms of the same frequency with identical phase angles in each cycle. However, the notion of phase synchronization has been introduced as an extension of classical Huygens' synchronization in the case of interacting chaotic systems if there is an integer relationship of frequency, such that the cyclic systems share a repeating sequence of phase angles over consecutive cycles. The results of the phase synchronization method are compared with those of the classical cross‐correlation method in cases in which cross‐correlation method shows linear spatial cross‐dependency, but the phase synchronization yields nonlinear spatial phase dependency. In the analyses, teleconnection patterns derived from phase synchronization are first calculated for raw and de‐seasoned data (by removing periodic components in the surface air temperature series) in year‐month scale and then for the data in seasonal‐scale (namely, winter, spring, summer and autumn). Teleconnection patterns calculated by phase synchronization improve the experiential intra‐phase relationships between the NCP Index (NCPI) and large‐scale surface air temperature series, and ensures that the major modes of mid and high Northern Hemisphere variability in climate are characterized. Statistically significant phase synchronization patterns related to geopotential dipole heights of the NCPI extending over Greenland, the Balkans, Caspian Sea basin, eastern Mediterranean, Turkey and ...
format Article in Journal/Newspaper
author Tatli, Hasan
spellingShingle Tatli, Hasan
Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
author_facet Tatli, Hasan
author_sort Tatli, Hasan
title Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
title_short Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
title_full Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
title_fullStr Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
title_full_unstemmed Synchronization between the North Sea–Caspian pattern (NCP) and surface air temperatures in NCEP
title_sort synchronization between the north sea–caspian pattern (ncp) and surface air temperatures in ncep
publisher Wiley
publishDate 2007
url http://dx.doi.org/10.1002/joc.1465
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1465
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1465
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_source International Journal of Climatology
volume 27, issue 9, page 1171-1187
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.1465
container_title International Journal of Climatology
container_volume 27
container_issue 9
container_start_page 1171
op_container_end_page 1187
_version_ 1800752714636853248